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www.solid-earth-discuss.net/3/527/2011/
doi:10.5194/sed-3-527-2011
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The 11 May 2011 earthquake at Lorca (SE Spain) viewed in a structural-tectonic context
1Department of Earth Sciences, Utrecht University, PO. Box 80.021, 3508 TA Utrecht, The Netherlands
2Fugro Engineers B.V., Leidschendam, The Netherlands
Abstract. The Lorca earthquake of 11 May 2011 in the Betic Cordillera of SE Spain occurred almost exactly on the Alhama de Murcia fault, a marked fault that forms part of a NE-SW trending belt of faults and thrusts. The fault belt is reminiscent of a strike-slip corridor, but recent structural studies have provided clear evidence for reverse motions on these faults. Focal mechanisms of the main earthquake but also of a foreshock are strikingly consistent with structural observations on the Alhama de Murcia fault. This strengthens the conclusion that, rather than a strike-slip fault, the fault is at present a contractional fault with an oblique reverse sense of motion, presumably in response to NW directed motion of Africa with respect to Europe.
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Notice on Discussion StatusCitation: Vissers, R. L. M. and Meijninger, B. M. L.: The 11 May 2011 earthquake at Lorca (SE Spain) viewed in a structural-tectonic context, Solid Earth Discuss., 3, 527-540, doi:10.5194/sed-3-527-2011, 2011. Bibtex EndNote Reference Manager XML
